Scoat Fell is a
fell
A fell (from Old Norse ''fell'', ''fjall'', "mountain"Falk and Torp (2006:161).) is a high and barren landscape feature, such as a mountain or Moorland, moor-covered hill. The term is most often employed in Fennoscandia, Iceland, the Isle of M ...
in the western part of the English
Lake District
The Lake District, also known as ''the Lakes'' or ''Lakeland'', is a mountainous region and National parks of the United Kingdom, national park in Cumbria, North West England. It is famous for its landscape, including its lakes, coast, and mou ...
. It stands at the head of the Mosedale Horseshoe with its back to Ennerdale. Paths lead to Scoat Fell from
Ennerdale over
Steeple, from
Wasdale over
Red Pike, and along the ridge from
Pillar.
Topography
The
Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and
Wasdale to the south east. Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are
Great Gable and its satellites, while two principal ridges fan out on either flank of
Ennerdale, the western fells in effect being a great horseshoe around this long wild valley.
Alfred Wainwright
Alfred Wainwright Order of the British Empire, MBE (17 January 1907 – 20 January 1991), who preferred to be known as A. Wainwright or A.W., was a British fellwalking, fellwalker, guidebook author and illustrator. His seven-volume ''Pictorial ...
: ''A Pictorial Guide to the Lakeland Fells, Volume 7 The Western Fells'': Westmorland Gazette (1966): Scoat Fell is on the southern arm.
The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and
Wasdale. The principal fells in this section are
Kirk Fell,
Pillar, Scoat Fell,
Haycock and
Caw Fell, followed by the lower
Lank Rigg group.
Scoat Fell occupies an important position at the crossroads of five ridges. To the east, across the subsidiary top of Black Crag, is Pillar. Southward is a long descending ridge heading toward the shore of Wastwater. The high point is
Red Pike, before the terminal height of
Yewbarrow. The main watershed continues west to Haycock, while two short spurs jut north into Ennerdale. These are Tewit How which descends from the western end of the plateau and
Steeple, running from the summit.
As the radial point of so many ridges Scoat Fell forms the head of several valleys, the major ones being the Wasdale feeders of Mosedale and Nether Beck. Mosedale begins on the eastern flanks of Scoat Fell, between Red Pike and Pillar, in the hollow of Black Comb. There are crags in the headwall, particularly to the south. Nether Beck has its birth at Scoat Tarn, a large pool to the south of the fell. This corrie
tarn, held in place by grassy
moraine
A moraine is any accumulation of unconsolidated debris (regolith and Rock (geology), rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a gla ...
s is around 65 ft deep.
[Blair, Don: ''Exploring Lakeland Tarns'': Lakeland Manor Press (2003): ] Between Steeple and Pillar to the north is Windgap Cove with Black Crag, a
Hewitt at its head. Wind Gap is the
col between Black Crag and Pillar, while the small Mirk Cove lies between Black Crag and the summit. Finally Mirklin Cove is the corrie between Steeple and Tewit How, drained into Ennerdale by Low Beck. All of the northern coves are home to impressive crags.
Of Scoat Fell's various satellites, Little Scoat Fell and Black Fell are generally considered to be a part of the parent fell, while Steeple, despite its clearly derivative position, is counted as a separate fell.
This is due to its impressive appearance from Ennerdale rather than any great
relative height
In topography, prominence or relative height (also referred to as autonomous height, and shoulder drop in US English, and drop in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling ...
, a triumph of the emotions over logic.
Geology
Successive rock strata are displayed along the descending ridge of Tewit How to the north west, displaying the architecture of the fell. At the top is the
plagioclase
Plagioclase ( ) is a series of Silicate minerals#Tectosilicates, tectosilicate (framework silicate) minerals within the feldspar group. Rather than referring to a particular mineral with a specific chemical composition, plagioclase is a continu ...
-phyric
andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predomina ...
lava
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a Natural satellite, moon onto its surface. Lava may be erupted at a volcano or through a Fissure vent, fractu ...
of the Birker Fell Formation, followed by the
siltstone,
sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sand ...
, conglomerate,
tuff and
lapilli tuff of the Eagle Crag Member. Further outcrops of the Birker Fell Formation are followed by a band of
dacite before the igneous rocks of the Ennerdale Intrusion complete the picture.
British Geological Survey
The British Geological Survey (BGS) is a partly publicly funded body which aims to advance Earth science, geoscientific knowledge of the United Kingdom landmass and its continental shelf by means of systematic surveying, monitoring and research. ...
: 1:50,000 series maps, ''England & Wales Sheet 29'': BGS (1999)
Summit
The top is a long plateau, running broadly east to west. Along it runs the stone wall of the Ennerdale fence, crossing the summit exactly. Purists have built a small
cairn
A cairn is a human-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the (plural ).
Cairns have been and are used for a broad variety of purposes. In prehistory, t ...
atop the wall, although a larger edifice lies just to the north, pointing the way to Steeple. The whole area is stony, with fine views into the northern coves.
Ordnance Survey
The Ordnance Survey (OS) is the national mapping agency for Great Britain. The agency's name indicates its original military purpose (see Artillery, ordnance and surveying), which was to map Scotland in the wake of the Jacobite rising of ...
maps label the summit as Little Scoat Fell and a small hillock at the western end of the plateau as Great Scoat Fell. These names are based on area rather than height, Great Scoat Fell being lower.
Pillar reduces the field of view, without showing its better side, but almost the full horseshoe of the Western Fells can be seen. The wall makes it difficult to observe the full panorama from one point.
Ascents
From Ennerdale many walkers will ascend indirectly via Steeple, but the ridge of Tewit How can also be used. Wasdale Head can be used as a base, first walking up Mosedale and then climbing up to the ridge via Black Comb. Finally Nether Beck Bridge on the shore of
Wastwater provides access via Scoat Tarn onto the southern flanks. From the upper recesses of Nether Beck the walker can aim for either of the cols which connect the objective to Red Pike or Haycock. Perhaps the greatest number of visitors will cross the top as part of the
Mosedale Horseshoe, also climbing Red Pike and Pillar.
[Bill Birkett:''Complete Lakeland Fells'': Collins Willow (1994): ]
References
{{Western Fells
Nuttalls
Hewitts of England
Fells of the Lake District
Cumberland (unitary authority)